Fractal Characteristics of Fault Structures and Their Use for Mapping Ore-prospecting Potential in the Qitianling Area, Southern Hunan Province, China     

WANG Nan  LIU Yongshun  PENG Nian  WU Cailai  LIU Ningqiang  NIE Baofeng  YANG Xiaoyu 《《地质学报》英文版》2015,89(1):121-132

Quantitative analyses of the spatial distribution of fault structures can provide a theoretical basis for forecasting prospective ore deposits. Characteristics and complexity of fault structure distribution in the Qitianling area, Southern Hunan Province, China, were quantitatively calculated and appraised by fractal and multifractal methods to evaluate the relation between fault structures and ore-prospecting potential. The results show that the lengths of faults can be modeled as multifractals. Multifractal spectra evidently reflect the characteristics of the scaling of fault structures. The boxcounting dimension value(D) of fault structures is equal to 1.656, as indicates complexity of the spatial distribution of faults and favorable structural conditions for the formation of ore deposits. Moreover, the D values of sub-regions were calculated and isopleths of their fractal dimension values were plotted accordingly. Overlay analyses of isopleths of fractal dimension values and distributions of known ore deposits show that areas with the larger fractal dimension values of fault structures have more ore deposits. This spatial coupling relationship between D values and ore deposits can be used to forecast and explore other ore deposits. On the basis of complexity theory for ore-forming systems, three exploration targets with high D values were delineated as prospective ore deposits.  相似文献   

Structural Characteristics of the Suoluogou Gold Deposit in Muli County, West Sichuan Province     

NIE Fei  FAN Wenyu  LIU Shusheng  ZHU Huaping  YANG Yongfei  SHI Hongzhao 《《地质学报》英文版》2015,89(5):1773-1774

<正>The Suoluogou gold deposit in Muli County of Sichuan Province is located in the southern section of the GanziLitang suture zone(Figs.1a,b),which is the largest gold deposit discovered in this suture zone in recent years.At present,the exploration of the Suoluogou gold deposit is still in progress,and the amount of resource is increasing.  相似文献   

湖南东南部湘东钨矿区老山坳断层性质的厘定及其对找矿的启示   总被引：1，自引：0，他引：1  

倪永进  单业华  伍式崇  聂冠军  张小琼  朱浩峰  梁新权 《大地构造与成矿学》2015,(3)

老山坳断层是湖南东南部湘东钨矿区的主干断层,目前有关其活动时代、性质和位移量的认识还存在分歧。断层带内及附近的宏观构造变形观察、断层两盘矿脉成分、结构构造和围岩变形的比较、岩石蚀变的类型和空间分布特征等都表明该断层具有正断性质,形成于成矿之后。鉴于下盘北组脉与上盘南南组脉具有平行脉壁、黑白相间的条带结构,认为它们在老山坳断层形成前应该属于同一组脉,进而推断出该断层的水平断距达1.5~2.0 km。无论单一脉或连接脉,矿脉的平均宽长比都大于1.0×10–2,远高于前人在露头上测量得到的石英脉宽长比,意味着脉体宽长比与观察的脉体尺度有关。在上述分析的基础上,提出新的找矿思路:在断层下盘北组脉的北边寻找与中组脉和南组脉对应的矿脉,而在断层上盘南南组脉的深部寻找北组脉。  相似文献   

一种BDS广播星历异常值实时探测方法     

卞艺潼  聂志喜  王振杰  徐晓飞  刘金萍 《大地测量与地球动力学》2022,42(11):1122-1127

针对BDS广播星历提出一种实时异常探测方法。首先通过检查广播星历参数是否超限来判断异常广播星历;然后计算相邻历元广播星历在中间时刻的空间信号测距差SISRD,基于广播星历的一致性进行异常值探测;最后对ALIC、AREG、ABMF、GENO测站的BDS广播星历数据进行异常探测,以最终精密星历探测结果作为参考进行验证。结果表明,该方法能够准确地探测出异常广播星历。  相似文献   

基于自适应UKF的BP神经网络及其在高程拟合中的应用     

聂建亮  秦勇  刘辉 《测绘科学》2007,32(6):120-122

针对BP神经网络收敛速度慢、容易陷入局部极小值点和泛化能力差等问题,基于自适应Kalman滤波理论,提出一种自适应非线性滤波(UKF)训练BP神经网络的方法。该方法采用Kalman滤波框架,引入自适应因子,对神经网络的连接权进行训练,提高了神经网络的学习质量。高程异常拟合算例表明,基于自适应UKF的BP神经网络比标准BP神经网络收敛速度快,泛化能力强,从而证明了该方法是一种有效的连接权训练方法。  相似文献   

面向灾害管理的自发地理信息研究及应用   总被引：1，自引：0，他引：1  

陈豪  张万昌  邓财  聂宁  易路 《测绘科学》2018,(1):59-65

针对目前自发地理信息(VGI)应用于灾害管理的巨大潜力和需求,该文系统地介绍了VGI应用于灾害管理中所面临的机遇及数据可用性、数据质量、数据管理和法律议题等方面的挑战;在此基础上,针对VGI数据质量问题,结合我国灾害管理实际情况,提出了3种提高VGI数据质量的方法,即VGI数据贡献者分类与权限设计、政府引导下的灾害管理VGI数据采集框架以及VGI数据质量评估体系;最后,以开发的地震灾情信息管理原型系统为例,讨论VGI应用于灾害管理中的数据采集框架、数据模型等关键技术问题,具有一定的推广和应用价值。  相似文献   

辐射产品的卫星影像内部畸变几何标定     

聂振钢  王鹏生 《测绘科学》2018,(2):101-107

针对卫星发射以后,由于外部太空环境的变化和相机光学系统的径向畸变导致卫星成像影像的外部误差和内部畸变,须对光学遥感相机长期周期性地进行几何标定消除卫星影像系统误差和相机指向角误差提高卫星影像几何定位精度的问题,该文从简单易行的角度出发,基于相机的CCD固定偏差原理构建一种新型的模型或内标定算法消除影像的内部畸变,以经过畸变改正的卫星影像辐射产品为参考控制,采用亚像素匹配法构建内部畸变模型修正卫星遥感影像的内部畸变,并分别以不同侧摆角和影像行数的SJ9A和ZY3为实验和参考控制数据构建和验证新型标定模型的有效性和实用性。  相似文献   

地表反射率数据库的构建及其应用     

聂振钢  王鹏生 《测绘科学》2018,(3):154-160

针对实现卫星对地观测的自适应多模态,需要根据先验判定卫星成像区域内地表覆盖类型及其反射率状况建立与太阳光照条件、地表覆盖类型、反射率相关的成像载荷积分时间、不同压缩比的成像参数设置模型,以选择最优的观测模式的问题,该文以中分辨率成像光谱仪(MERIS)地表反射率影像和GlobCover全球陆地覆盖分类图为数据源,建立了地表覆盖分类图及其反射率影像矢量化处理的技术流程,构建了以冰雪、沙漠、裸土、岩石、农作物、森林、草地、水体等不同地表覆盖类型及其在不同季节蓝、绿、红、近红外波段的地物反射率数据库。以此作为遥感卫星成像任务规划的技术支撑,构建自适应选择最优的观测模式,提升遥感图像的质量。  相似文献   

Zircon U–Pb Geochronology and Petrogenesis of Early–Midlle Permian Arc–Related Volcanic Rocks in Central Jilin: Implications for the Tectonic Evolution of the Eastern Segment of Central Asian Orogenic Belt     

SHI Chenglong  DING Xiaozhong  LIU Yanxue  ZHOU Xiaodong  NIE Lijun 《《地质学报》英文版》2020,94(4):1207-1222

This paper presents age and geochemical data of a recently identified Late Paleozoic volcanic sequence in central Jilin Province, with aims to discuss the petrogenesis and to constrain the tectonic evolution of the Central Asian Orogenic Belt in this area. Firstly, the volcanic rocks have zircon U-Pb ages of 290–270 Ma. Secondly, they are characterized by(a) ranging in composition from the low-K tholeiite series to high-K calc-alkaline series;(b) enrichment in light rare earth elements and depletion of heavy rare earth elements, with negative Eu anomalies; and(c) negative Nb, Ta, and Ti anomalies. Finally, the volcanic rocks yield εHf(t) values of +7.1 to +17. These data suggest that the central Jilin volcanic rocks were possibly derived from predominant partial melting of a depleted lithospheric mantle that might have been modified by subducted slab–derived fluids. Combined with previous studies, the Late Paleozoic–Early Mesozoic magmatism in Central Jilin can be divided into two stages:(a) a volcanic arc stage(290–270 Ma) represented by low-K to high–K, tholeiite to calc–alkaline plutons and(b) a syn–collisional stage(260–240 Ma) represented by high-K calc–alkaline I-type granites. Furthermore, the timing and the tectonic setting of the above magmatic rocks show that the arc was probably produced by the northward subduction of the Paleo-Asian Ocean and that the final closure of the Paleo-Asian Ocean occurred prior to the Early Triassic.  相似文献   

Late Paleozoic Element Migration and Accumulation under Intracontinental Sinistral Strike-slip Faulting in the West Junggar Orogenic Belt, NW China     

WANG Ye  CHEN Xuanhu  NIE Lanshi  DING Weicui  WANG Xueqiu  XU Shenglin  MA Feizhou  HAN Lele 《《地质学报》英文版》2020,94(6):2012-2030

The migration, accumulation and dispersion of elements caused by tectonic dynamics have always been a focus of attention, and become the basis of tectono-geochemistry. However, the effects of faulting, especially strike-slip faulting, on the adjustment of geochemical element distribution, are still not clear. In this paper, we select the West Junggar Orogenic Belt (WJOB), NW China, as a case study to test the migration behavior of elements under tectonic dynamics. The WJOB is dominated by NE-trending large-scale sinistral strike-slip faults such as the Darabut Fault, the Mayile Fault, and the Baerluke Fault, which formed during the intracontinental adjustment under N–S compression during ocean-continental conversion in the Late Paleozoic. Geochemical maps of 13 elements, Al, W, Sn, Mo, Cu, Pb, Zn, As, Sb, Hg, Fe, Ni, and Au, are analyzed for the effects of faulting and folding on element distribution at the regional scale. The results show that the element distribution in the WJOB is controlled mainly by two mechanisms during tectonic deformation: first is the material transporting mechanism, where the movement of geological units is consistent with the direction of tectonic movement; second is the diffusion mechanism, especially by tectonic pressure dissolution driven by tectonic dynamics, where the migration of elements is approximately perpendicular or opposite to the direction of tectonic movement. We conclude that the adjustment of element distributions has been determined by the combined actions of transporting and diffusion mechanisms, and that the diffusion mechanism plays an important role in the formation of geochemical Au blocks in the WJOB.  相似文献